One explanation could be summer surface melt water that acted like a wedge on small cracks, eventually opening them into a large rift.

The Roman poet Ovid once quipped that "dripping water hollows out stone, not through force but through persistence."

When it comes to buckling ancient, thousand-foot-thick ice shelves — and perhaps the 1.1-trillion-ton, Delaware-size piece of ice that Antarctica just shed into the sea— Ovid may have been wise beyond his years.

A 300-foot-wide, 70-mile-long rift in Antarctica's Larsen C ice shelf, as seen in November 2016. John Sonntag/IceBridge/NASA Goddard Space Flight Center The iceberg, dubbed A68 by the US National Ice Center, took years to form as the result of a crack in the Larsen C ice shelf. The crack formed around 2010 but grew rapidly starting in 2016.

While the world watches it slowly disintegrate, many are left wondering: What caused the iceberg to break off?

"There are lots of reasons," Martin O'Leary, a glaciologist with Swansea University and the Antarctic research program Project Midas, wrote in a Reddit ask-me-anything session on July 14. "[E]ither something is pulling the ice apart, or something has got into a gap and is pushing it open."

A liquid wedge

One driving, Ovid-like force may be similar to what doomed Larsen B, a nearby ice shelf on the Antarctic Peninsula. Over the past 50 years, this region has experienced warming that is three times greater than the global average.

In 2002, scientists looked on as nearly the entire Larsen B ice shelf fell into the sea after a large piece calved into the Southern Ocean.

"For events like the breakup of Larsen B, it was melt water filling all the surface cracks and [slowly] pushing them open," he said. (Melt water that appears primarily in the summer can sink into and weaken ice shelves over several seasons.)

Surface melt water on East Antarctica's Amery Ice Shelf, as seen by NASA's Landsat 4 satellite. NASA/MODIS

"In places like Alaska you often get ocean water undercutting a glacier," he added, "which destabilizes the ice at the front, and it gets pulled apart by gravity."

O'Leary said no one can be certain what caused iceberg A68 to break off, or at least yet; it's far too cold in the Antarctic winter to fly in a crack research team. We may have to wait until November, when the southern hemisphere waxes toward summer and it becomes safe to fly airplanes over Antarctica again.

"We've got some theories, but nothing that we've got good evidence for," he said. "Icebergs like this are so rare that it's hard to develop any kind of comprehensive theory — you end up focusing on the details of each individual berg."

How much are humans to blame?

Scientists say this particular calving won't raise sea levels, since the ice was already floating in the water. (The effect is similar to why melting ice cubes in a drink don't overflow a glass.)

O'Leary and his colleague Adrian Luckman, who's also with Swansea University and Project Midas, previously suggested that A68's calving was " a natural event". After all, ice shelves have been cracking off huge icebergs for eons.

Iceberg B-15A was a fragment of iceberg B-15, the largest ever recorded with a surface are of 4,200 square miles (11,00 square kilometers).Josh Landis/NSF

Yet other scientists say this perspective is akin looking at the situation "through a microscope" instead of acknowledging the bigger, inevitable picture of human-driven global warming and climate change.

"To me, it's an unequivocal signature of the impact of climate change on Larsen C," Eric Rignot, a glaciologist at NASA JPL, told writer John D. Sutter for a July 15 column at CNN. "This is not a natural cycle. This is the response of the system to a warmer climate from the top and from the bottom. Nothing else can cause this."

While the debate over A68 continues, so does the seemingly uninterruptible march of climate change and its disruptive and potentially disastrous effects.